Preface to integrative stratigraphy, biotas, and paleogeographical evolution of the Qinghai-Tibetan Plateau and its surrounding areas

Diffusion-induced lithium isotopic heterogeneity in olivines from peridotites of an oceanized mantle lithosphere at the Yunzhug ophiolite (central Tibet)

Plant compartment niche is more important in structuring the fungal community associated with alpine herbs in the subnival belt of the Qiangyong glacier than plant species

Assessing hydrothermal changes in the upper Yellow River Basin amidst permafrost degradation

Nature-based Solutions can help restore degraded grasslands and increase carbon sequestration in the Tibetan Plateau

Can inter-annual climate variability alone explain the glacier retreat since the Little Ice Age in the Hailuogou catchment, southeastern Tibetan Plateau?